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Diamonds are highly prized for their qualities but also for their rarity. The necessary conditions to form diamond at great depths in the Earth’s mantle are only met in a few places. The geographic distribution of diamonds is very uneven, with notable concentrations in Africa, Brazil, Canada, India and Siberia. All of these places are characterised by ancient continental crust between 2.5 and 3.5 billion years old.
This crust is underlain by deep solid 'roots' made of mantle which has become highly chemically depleted through intense melting over time. It’s here in this depleted mantle, which extends as deep as 250 km into the hotter, stirring mantle below it, that diamonds have the best opportunity to form.
the 4 Cs
Year | Carats |
---|---|
1971 | 6.6 |
1987 | 11.1 |
1990 | 14.2 |
the 4 Cs
Cost is the fifth 'C'
The Tolkowsky design was slightly modified to become the Standard Round Brilliant (SRB), widely used today.
Carat | Diameter (mm) |
Height (mm) |
---|---|---|
0.10 | 2.98 | 1.67 |
0.25 | 4.04 | 2.26 |
0.50 | 5.09 | 2.85 |
0.75 | 5.83 | 3.27 |
1.00 | 6.42 | 3.60 |
1.25 | 6.91 | 3.80 |
1.50 | 7.35 | 4.12 |
1.75 | 7.74 | 4.33 |
2.00 | 8.09 | 4.54 |
2.50 | 8.71 | 4.88 |
3.00 | 9.25 | 5.19 |